Spatial Scale and Field Management Affect Patterns of Phosphorus Loss in Cranberry Floodwaters

Although cranberries ( Vaccinium macrocarpon Ait.) are indigenous to the northeastern United States, phosphorus (P) fertilizer additions and periodic flooding make commercial cranberry a potential source of P to the region's lakes and streams. In this study, we report values of P export in cranberry floodwaters that range from <0.8 to 4.7 kg P ha −1 , generally reflecting differences in the hydrological, edaphic, and management factors underlying soil P transfer to floodwater. The relatively high P loading rate (4.7 P kg P ha −1 ) was associated with harvest flooding of organic‐rich soils. Periods of winter flooding and the discharge of harvest floodwater from mineral soils resulted in relatively low P loss (<0.8 kg P ha −1 ). Increases in concentrations of total dissolved P (DP) and total particulate P (PP) in floodwater as stage decreased below the surface of the cranberry bed were consistent with the transport of dissolved P in soil porewater and mobilization of particulate P in ditches. Variations in floodwater DP, as well as conservative and reactive tracer concentrations, suggested that the processes by which soil P is released to porewater included desorption of near‐surface soil P and anaerobic dissolution of iron‐P compounds deeper in the soil profile. At the farm scale, concentrations of DP and PP steadily increased over time, presumably because drainage waters from beds farther upgradient had longer contact times with P‐rich sources, such as soil porewater and ditch sediments. Overall, the study illustrates the role that scale‐dependent processes impart on patterns of P loss in agricultural production systems. Core Ideas Relatively high P loss was associated with the harvest flood rather than the winter flood. Recently renovated farms exhibited lower values of P export in floodwater. Soil porewater that was high in P was discharged later in the flood release.